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孟加拉湾热带风暴对青藏高原降水和土壤湿度的影响

DOI: 10.1007/s11430-014-5028-8, PP. 625-638

Keywords: 热带风暴,孟加拉湾,青藏高原,土壤湿度,积雪,WRF模式

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Abstract:

?利用JTWC提供的1981~2011年孟加拉湾热带风暴最佳路径资料,研究春季、初夏(AMJ)及秋冬季节(SOND)孟加拉湾风暴对青藏高原降水及土壤湿度的影响特征.研究表明:每年平均约1.35个孟加拉湾风暴能够影响青藏高原,5和10月是孟加拉湾风暴影响青藏高原的两个主要时期,且在AMJ生成的风暴比SOND影响范围更大,影响的纬度更偏北;孟加拉湾风暴引起的降水最大可超过当地当月降水量的50%,同时也能够占到整个季节的20%.资料分析还表明春季风暴降水引起的青藏高原表层土壤湿度异常大概能维持20~25d,秋冬季节孟加拉湾风暴引起的高原积雪也仅能维持20d左右便基本消融殆尽.数值试验表明青藏高原表层土壤湿度异常仅持续20d左右,次表层异常则大概可以持续2个月,而更深层次土壤湿度异常则可维持数个月甚至更久.最后,统计关系还表明前期风暴引起的高原积雪及土壤湿度异常并不足以影响到东亚夏季降水,其与中国东部夏季降水异常无直接联系.近30年来孟加拉湾风暴强度增强,使得20世纪90年代中期以后孟加拉湾风暴对青藏高原春季降水的影响有所增强.

References

[1]  北京大学地球物理系热带天气研究组, 国家海洋局预报总台热带天气预报研究组. 1974. 孟加拉湾风暴的活动及其对我国天气的影响. 气象科技, 2: 3-22
[2]  陈烈庭. 1998. 青藏高原冬春季异常雪盖与江南前汛期降水关系的检验和应用. 应用气象学报, 9(增刊): 1-8
[3]  戴武杰. 1974. 孟加拉湾台风对西藏高原的影响. 气象, 4: 12-13
[4]  段安民, 刘屹岷, 吴国雄. 2003. 4~6月青藏高原热状况与盛夏东亚降水和大气环流的异常. 中国科学D辑: 地球科学, 33: 997-1004
[5]  段旭, 陶云, 寸灿琼, 等. 2009. 孟加拉湾风暴时空分布和活动规律统计特征. 高原气象, 28: 634-641
[6]  丁一汇. 1975. 西藏高原的云图分析. 陶诗言. 卫星云图使用手册(第3章). 北京: 中国农业出版社. 92-123
[7]  丁一汇. 1976. 南支槽与台风高空流场的相互作用及其对天气的影响. 全国气象卫星云图接收应用会议文集. 北京: 科学出版社. 127-142
[8]  李崇银, 刘会荣, 宋洁. 2013. 2009/2010年冬季云南干旱的进一步研究——前期土壤湿度影响的数值模拟. 气候与环境研究, 18: 551-561
[9]  罗会邦, 陈蓉. 1995. 夏半年青藏高原东部大气热源异常对环流和降水的影响. 气象科学, 15: 94-102
[10]  彭雯, 高艳红, 王婉昭. 2012. 土壤温湿状况对黄河源区水循环过程的影响. 地球科学进展, 27: 1252-1261
[11]  彭雯, 高艳红. 2011. 青藏高原融冻过程中能量和水分循环的模拟研究. 冰川冻土, 33: 364-373
[12]  王曼, 段旭, 李华宏, 等. 2011. 孟加拉湾风暴Mala登陆期间地形敏感试验. 气象学报, 69: 486-495
[13]  王允宽, 刘俊清, 黄中华. 1986. 青藏高原地形对孟加拉湾热带气旋动力影响的模拟实验研究. 大气科学, 10: 27-37
[14]  王子谦, 朱伟军, 段安民. 2010. 孟湾风暴影响高原暴雪的个例分析: 基于倾斜涡度发展的研究. 高原气象, 29: 703-11
[15]  许美玲, 段旭, 张秀年. 2006. 登陆孟湾风暴结构演变特征数值模拟研究. 高原气象, 25: 1139-1146
[16]  Jones R H. 1975. Estimating the variance of time averages. J Appl Meteorol, 14: 159-163
[17]  Kim E J, Hong S Y. 2010. Impact of air-sea interaction on East Asian summer monsoon climate in WRF. J Geophys Res, 115: D19118
[18]  Kim J H, Wu C C, Sui C H, et al. 2012. Tropical cyclone contribution to interdecadal change in summer rainfall over South China in the early 1990s. Terr Atmos Ocean Sci, 23: 49-58
[19]  Kim Y, Wang G. 2007. Impact of initial soil moisture anomalies on subsequent precipitation over North America in the coupled land-atmosphere model CAM3-CLM3. J Hydrometeor, 8: 513-533
[20]  Kubota H, Wang B. 2009. How much do tropical cyclones affect seasonal and interannual rainfall variability over the western North Pacific? J Clim, 22: 5495-5510
[21]  Li Z, Yu W, Li T, et al. 2013. Bimodal character of cyclone climatology in the Bay of Bengal modulated by monsoon seasonal cycle. J Clim, 26: 1033-1046
[22]  Maussion F, Scherer D, Finkelnburg R, et al. 2011. WRF simulation of a precipitation event over the Tibetan Plateau, China—An assessment using remote sensing and ground observations. Hydrol Earth Syst Sci, 15: 1795-1817
[23]  Meng L, Long D, Quiring S M, et al. 2013. Statistical analysis of the relationship between spring soil moisture and summer precipitation in East China. Int J Climatol, doi: 10.1002/joc.3780
[24]  Paul B. 2010. Human injuries caused by Bangladesh''s cyclone Sidr: An empirical study. Nat Hazards, 54: 483-495
[25]  Qian Y F, Zheng Y Q, Zhang Y, et al. 2003. Responses of China''s summer monsoon climate to snow anomaly over the Tibetan Plateau. Int J Climatol, 23: 593-613
[26]  Rao V B, Ferreira C C, Franchito S H, et al. 2008. In a changing climate weakening tropical easterly jet induces more violent tropical storms over the north Indian Ocean. Geophy Res Lett, 35: L15710, doi: 10.1029/2008GL034729
[27]  Ren F M, Gleason B, Easterling D. 2002. Typhoon impacts on China''s precipitation during 1957-1996. Adv Atmos Sci, 19: 943-952
[28]  Ren F M, Wang Y M, Wang X L, et al. 2007. Estimating tropical cyclone precipitation from station observations. Adv Atmos Sci, 24: 700-711
[29]  Ren F M, Wu G X, Dong W J, et al. 2006. Changes in tropical cyclone precipitation over China. Geophys Res Lett, 33: L20702, doi: 10.1029/2006GL027951
[30]  Rodell M, Houser P R, Jambor U, et al. 2004. The global land data assimilation system. Bull Amer Meteor Soc, 85: 381-394
[31]  Rowntreen P R, Bolton J A. 1983. Simulation of the atmospheric response to soil moisture anomalies over Europe. Quart J Roy Meteor Soc, 109: 501-526
[32]  Seol K H, Hong S Y. 2009. Relationship between the Tibetan snow in spring and the East Asian summer monsoon in 2003: A global and regional modeling Study. J Clim, 22: 2095-2110
[33]  Singh O P, Khan T M A, Rahman M S. 2001. Has the frequency of intense tropical cyclones increased in the north Indian Ocean? Curr Sci, 80: 575-580
[34]  Wang Z Q, Duan A M, Wu G X. 2013. Time-lagged impact of spring sensible heat over the Tibetan Plateau on the summer rainfall anomaly in East China: Case studies using the WRF model. Clim Dyn, doi: 10.1007/s00382-013-1800-2
[35]  Wu T W, Qian Z A. 2003. The relation between the Tibetan winter snow and the Asian summer monsoon and rainfall: An observational investigation. J Clim, 16: 2038-2051
[36]  Wu W R, Dickinson R E. 2004. Time scales of layered soil moisture memory in the context of land-atmosphere interaction. J Clim, 17: 2752-2764
[37]  Wu Y J, Wu S G, Zhai P M. 2007. The impact of tropical cyclones on Hainan Island''s extreme and total precipitation. Int J Clim, 27: 1059-1064
[38]  Yeh T C, Weatherald R T, Manabe S. 1984. The effect of soil moisture on short-term climate and hydrology change-a numerical experiment. Mon Weather Rev, 112: 474-490
[39]  赵平, 陈隆勋. 2001. 35年来青藏高原大气热源气候特征及其与中国降水的关系. 中国科学D辑: 地球科学, 31: 327-332
[40]  张顺利, 陶诗言. 2001. 青藏高原积雪对亚洲夏季风影响的诊断及数值研究. 大气科学, 25: 372-390
[41]  周倩, 王式功, 尚可政, 等. 2011. 2008年10月青藏高原东部一次区域暴雪过程及气候背景分析. 高原气象, 30: 22-29
[42]  朱福康, 郑新江, 罗敬宁, 等. 1998. 藏南暴雪过程的水汽图像. 科学通报, 43: 2232-2235
[43]  朱玉祥, 丁一汇, 徐怀刚. 2007. 青藏高原大气热源和冬春积雪与中国东部降水的年代际变化关系. 气象学报, 65: 946-958
[44]  Alam M M, Hossain M A, Shafee S. 2003. Frequency of Bay of Bengal cyclonic storms and depressions crossing different coastal zones. Int J Climatol, 23: 1119-1125
[45]  Atkinson G D. 1971. Forecasters'' guide to tropical meteorology. Air Weather Service, MAC, United States Air Force. 240
[46]  Bern C, Sniezek J, Mathbor G M, et al. 1993. Risk factors for mortality in the Bangladesh cyclone of 1991. Bull World Health Organ, 71: 73-78
[47]  Chen J M, Li T, Shih C F. 2010. Tropical cyclone- and monsoon-induced rainfall variability in Taiwan. J Clim, 23: 4107-4120
[48]  Chen Y Y, Yang K, Qin J, et al. 2013. Evaluation of AMSR-E retrievals and GLDAS simulations against observations of a soil moisture network on the central Tibetan Plateau. J Geophys Res, 118: 4466-4475
[49]  Chu J H, Sampson C R, Levine A S, et al. 2002. The joint typhoon warning center tropical cyclone best-tracks, 1945-2000. Naval Research Laboratory Tech Rep. 112
[50]  Dee D P, Uppala S M, Simmons A J, et al. 2011. The ERA-Interim reanalysis: Configuration and performance of the data assimilation system. Quart J Roy Meteor Soc, 137: 553-597
[51]  Delworth T L, Manabe S. 1988. The influence of potential evaporation on the variabilities of simulated soil wetness and climate. J Clim, 1: 523-547
[52]  Duan A M, Wu G X. 2008. Weakening trend in the atmospheric heat source over the Tibetan Plateau during recent decades. Part I: Observations. J Clim, 21: 3149-3164
[53]  Entin J K, Robock A, Vinnikov K Y, et al. 2000. Temporal and spatial scales of observed soil moisture variations in the extratropics. J Geophys Res, 105: 11865-11877
[54]  Gray W M. 1968. Global view of the origin of tropical disturbances and storms. Mon Weather Rev, 96: 669-700
[55]  Huffman G J, Adler R F, Bolvin D T, et al. 2007. The TRMM multisatellite precipitation analysis (TMPA): Quasi-global, multiyear, combined-sensor precipitation estimates at fine scales. J Hydrometeor, 8: 38-55

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